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- W201693911 abstract "Mesozoic extension of the Grand Banks and Orphan provinces and their surrounding conjugate margins was accommodated by a system of intracrustal detachments. Late Jurassic-Early Cretaceous subsidence occurred above a down-to-the-west intracrustal detachment that is ~26 km deep beneath the Jeanne d'Arc basin. The structural styles and stratigraphy are intermittently linked to this history of crustal dynamics and sequential ocean opening. The late Callovian onset of extension was a widespread argillaceous sag unattended by significant faulting. The climax of basin subsidence in the late Kimmeridgian-early Valanginian was fault controlled and characterized by high structural relief that formed a closed fluvial-dominated basin system. During late Valanginian-Aptian time, syndepositional normal faulting was less intense, and the shallow marine paleogeography spilled across the rift shoulders. A later episode of mid-Aptian through Cenomanian NE-directed extension, accompanied by mantle flow, created the conspicuous northward axial-plunge of the basin and accounts for the maximum thickness, up to 18 km, of the basin fill. Restoration of these extensional tracts suggests a three-dimensional control of overlapping crustal plates to explain structural-stratigraphic evolution of the Jeanne d'Arc basin." @default.
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- W201693911 date "2012-01-01" @default.
- W201693911 modified "2023-09-27" @default.
- W201693911 title "Extensional tectonics and stratigraphy of the Mesozoic Jeanne d'Arc basin, Grand Banks of Newfoundland" @default.
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- W201693911 doi "https://doi.org/10.1016/b978-0-444-56356-9.00013-4" @default.
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